Phycosphere pH of unicellular nano- and micro- phytoplankton cells and consequences for iron speciation

Surface ocean pH is declining due to anthropogenic atmospheric CO(2) uptake with a global decline of ~0.3 possible by 2100. Extracellular pH influences a range of biological processes, including nutrient uptake, calcification and silicification. However, there are poor constraints on how pH levels i...

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Detalles Bibliográficos
Autores principales: Liu, Fengjie, Gledhill, Martha, Tan, Qiao-Guo, Zhu, Kechen, Zhang, Qiong, Salaün, Pascal, Tagliabue, Alessandro, Zhang, Yanjun, Weiss, Dominik, Achterberg, Eric P., Korchev, Yuri
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9478132/
https://www.ncbi.nlm.nih.gov/pubmed/35798938
http://dx.doi.org/10.1038/s41396-022-01280-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9478132/
https://www.ncbi.nlm.nih.gov/pubmed/35798938
http://dx.doi.org/10.1038/s41396-022-01280-1

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